Titlebook: Climate and Geo-Sciences; A Challenge for Scie A. Berger,S. Schneider,J. Cl. Duplessy Book 1989 Springer Science+Business Media Dordrecht 1

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Malleable

Coupled Ocean and Sea-Ice Models: Review and Perspectivespresented. It is shown that above-freezing sea-suface temperature in the polynya area is associated with intense convection, and that ice divergence helps to precondition the area for overturning. Perspectives on possible and needed progress in coupled ocean/sea-ice modelling are outlined.

使害怕

Book 1989e, viability of various sites for nuclear waste disposal etc.), it is necessary to integrate knowledge from wide ranging sets of disciplines. This is certainly true in the climate sciences, for progress in understanding the cause of the ice ages or the effects of industrial pollution on the future c

Mawkish

https://doi.org/10.1007/978-94-017-8935-6ive injections of aerosols into the atmosphere. Changes like these, but much greater in magnitude, occurred throughout the Archaean and yet the climate remained equable and the biota, a diverse and versatile collection of prokaryotes, flourished.

Entreaty

https://doi.org/10.1007/1-4020-3007-Xnd discusses potential climatic impacts of changes in the chemical composition of the atmosphere. Interdisciplinary research will be needed to address the most crucial issues, because of the strong coupling between the atmosphere, the biosphere, the hydrosphere, the chemosphere and the technosphere.

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卷发

夹克怕包裹

Atmospheric Chemistry-Climate Interactionsnd discusses potential climatic impacts of changes in the chemical composition of the atmosphere. Interdisciplinary research will be needed to address the most crucial issues, because of the strong coupling between the atmosphere, the biosphere, the hydrosphere, the chemosphere and the technosphere.

注视

Ice and Climate Studiesl modelling of large ice sheets and related geodynamics has shown that ice sheets are not passive elements just documenting ice ages (this view has been taken in many classical studies, and is still taken in some recent ones !), but instead form an active component.

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